The Boeing 707, 727, and Douglas DC8 era jets were rarely flying above 35,000 and usually 31,000 to 33,000. Today a 737, 767, or AirBus will routinely fly at 41,000 and burn 50% less fuel. The jet-stream is associated with the tropopause, which is the boundary between the stratosphere and the troposphere, and normally starts around 36,000 and is 4,000 to 6,000 thick. Wind, temp, and pressure are what determine the density and dissipation of contrails. If contrails do, in fact last longer today, that may have something to do with it....or it could be those tanks filled with thousands of gallons of globally warmed and fermented bovine flatulation that airlines spray from secret cargo compartments to create holes in the ozone...who really knows?
Steve